Monsoon dynamics: △p -land-se 16 Thermal contrast: 0 SP E0 NP 4000 strength of circulation threshold of strong A)STREAMFUNCTION RUN N25T40 DAY 300 16 cross-equator meridional overturning (WX) 2000 circulation strong heating: 30 SIN (LATITUDE) e.(K) A)STREAMFUNCTION RUN N25T10 DAY 200 Plumb and Hou(1992) (Nx) weak heating: Numerical results for axisymmetric flow 305 SIN (LATITUDE) 30N 授课教师：张洋7授课教师：张洋 7 Monsoon dynamics: -land-sea contrast n Thermal contrast: Plumb and Hou (1992) Numerical results for axisymmetric flow weak heating: strong heating: threshold of strong cross-equator meridional overturning circulation strength of circulation